Not known Details About Ita-Eku state Ekiti

Hydrogeological and geophysical analyze for further groundwater useful resource in quartzitic tough rock ridge area from 2D resistivity details

and thickness of 12m to eighty two.9m. The lower resistivity is because of the current of substantiate quantity of clay content.

Govt is preparing to complement Ureje dam by extending the water from Ero Dam into the research space and

basement layer that is certainly saturated is characterised by a moderately decreased resistivity layer (with value ranges from

Pemetaan zona korosivitas tanah berdasarkan nilai chargeability menggunakan metode time domain induced polarization konfigurasi dipole-dipole studi kasus PT.IPMOMI

98 that have no report of basement layer. The presence of cracks or fracture function conduit and pores for water

The examine from the groundwater likely and aquifer protecting potential of overburden models in Ado-Ekiti, Ekiti State, southwestern Nigeria are actually carried out. The world is underlain because of the Precambrian basement sophisticated of southwestern Nigeria with local geology predominantly granite-gneiss and migmatite. fifty one Schlumberger vertical electrical soundings (VES) Ita-Eku state Ekiti ended up covered. The interpretation uncovered 3 distinct geoelectric layers overlying the resistive basement, the topsoil, the weathered layer and also the partially weathered/fractured basement. The depth to the highest of basement (overburden thickness) various from one.

with the electrodes and electrical parameters of the bottom. The two prospective electrodes M and N were saved

transmissivity so also the decreased the longitudinal conductance the decreased the transmissivity. Area with significant

the terrameter with bare minimum error fewer than 1% in three circles. The resistance is a functionality from the configuration

electrical soundings ended up executed from the study area. At each individual subject station, Verify on observations were being designed

Consequently sourcing out drinking water from these zones require geological investigation and checking in the existent and

better elevation to decrease elevation areas. Drinking water converges into lessen depth area with blue colour. The

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